Images

A telephoto image of fissures that opened on the western wall of Halema'uma'u crater during the ongoing eruption that began yesterday, September 29, at approximately 3:21 p.m. HST. Lava from multiple fissures continues to slowly raise the level of the new active lava lake at the summit of Kīlauea. USGS image by M. Patrick.

A telephoto image of one of the low lava fountains near the center of the growing Halema'uma'u lava lake. The ongoing eruption at the summit of Kīlauea is confined within Halema'uma'u, with numerous lava fountains producing lava and volcanic gases.

Hawaiian Volcano Observatory geologists collect tephra samples from the recent eruption within Halema'uma'u, at Kīlauea summit.  Geochemical analyses of these eruption products will provide information about magma storage prior to the eruption. USGS image by K. Lynn. 

Tephra from the recent eruption within Halema'uma'u, at Kīlauea summit, is accumulating downwind of the active vents. Tephra is a term that describes products of an eruption that travel through the air before being deposited.

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This timelapse image sequence shows the opening sequence of the new eruption in Halema‘uma‘u crater, at the summit of Kīlauea. The first few moments are shown on a loop several times to highlight the visible uplift of the crater floor, just before the appearance of new fissures.

This image from the northwest rim of Halema'uma'u crater was taken in the late morning on September 29, 2021, just a few hours before the new Kīlauea summit eruption began. The solidified lava lake (center) was emplaced between December 2020 and May 2021. USGS photo taken by L. Gallant.

KWcam image taken on September 28, 2021, before the eruption began in Halemaʻumaʻu on September 29, 2021.  Several islands, including the one in the center of the crater that formed on December 20, 2020, are surrounded by younger lava flows erupted during the December 2020-May 2021 Kīlauea summit eruption. USGS photo.

A view looking north into Halema‘uma‘u, at Kīlauea's summit, on September 24, 2021, seen during a brief clear spell between passing rain clouds. There has been no significant change in the surface elevation of the solidified crust of the lava lake since the eruption paused in late May 2021.

A paint brush is very useful to discern individual Kulanaokuaiki Tephra units by clearing away overlying younger ash and Pele's hair. At this field site on the south flank of Kīlauea, the Kulanaokuaiki Tephra is overlain by Observatory Shield lava flows and underlain by the Kīpuka Nēnē lava flows.

No changes were observed at Kīlauea's summit during a brief field visit on September 3, 2021. Sunny weather made for spectacular views, though strong winds were blowing. The solidified crust of the lava lake within Halema‘uma‘u—which was active from December 2020 to May 2021—is visible in the lower center of this image. USGS photo by K. Mulliken.

View from a temporary webcam, which is located just southwest of Kīlauea summit caldera, and looks south over the area of the August 2021 intrusion. The dark lava flow on the left of image (mid-ground) is where the 1982 lava flow spilled out of the south caldera.

An HVO scientist clears tephra from a solar panel during the September 2021 Kīlauea summit eruption. A glove is used to brush away the Pele’s hair and other fine volcanic glass fragments to avoid small cuts and splinters.

View to the southwest from HVO station HRPKE, showing Pu‘ukoa‘e on Kīlauea's Southwest Rift Zone in the background.

Station HRPKE is located southwest of Kīlauea's summit, in the upper Southwest Rift Zone region, within Hawai‘i Volcanoes National Park. The station measures sulfur dioxide (SO₂) concentrations in the air, as well as local meteorological data such as wind speed, wind direction, and rainfall.

On August 31, the water level in Keller Well was measured at approximately 514.12 m (1686.75 ft) below the ground surface. Though an intrusion of magma took place beneath the ground surface in Kīlauea's south caldera region from August 23–30, water level in Keller Well does not show significant changes as a result of this event. USGS image by P. Nadeau.

On Tuesday, August 31, Hawaiian Volcano Observatory (HVO) scientists and technicians visited the Keller Well in Kīlauea's south caldera region. Water from the well is typically sampled and analyzed quarterly to monitor how magma supply to Kīlauea's summit reservoirs might impact regional ground water.

This map depicts the detected intrusive activity over the past week at Kīlauea Volcano. The initial swarm of small earthquakes from August 23–25 was centered in the south caldera region, as labelled on the map.

Map showing the seismic activity beneath the south part of Kīlauea caldera, within Hawaiʻi Volcanoes National Park, from August 23, 2021, at noon through the same time on August 25, 2021. The earthquake swarm began in that region at around 4:30 p.m. HST on August 23 and continued until the morning of August 25, 2021.

On the north margin of the south sulfur bank, which was exposed during the Kīlauea summit collapse events in 2018, light-colored deposits are evidence of the ongoing alteration from volcanic gas emissions.

An HVO scientist uses a syringe to capture a sample from an area within Kīlauea caldera that was identified as emitting elevated levels of the volcanic gas carbon dioxide. The sample is transferred to a gas sample bag, which will later be taken to a lab for chemical analyses. USGS photo by K. Mulliken on August 3, 2021.